Several measuring methods using various properties of radar signals to
estimate rainfall rate R are reviewed. These methods are based on mea
surements of the radar reflectivity factor Z at one or two polarizatio
ns, on measurements of attenuation A or on a combination of these two
quantities. When only one radar observable is measured, R is computed
from analytical relations of R-Z or A-Z type, ignoring the spatiotempo
ral variations of the raindrop size distribution N(D), where D is the
drop diameter. If N(D) can be approximated by a two parameter equation
, R can be estimated from the determination of N(D), using measurement
s of two radar observables. Some of these methods are notably improved
if the radar data are combined with rain gauge network measurements a
t the ground. The mean volume rainfall and the areally averaged rain r
ate can be estimated from the area-time integral and fractional area m
ethods.